Compositional Characteristic and Petrogenic Feaures of Metasedimenary Rocks of Zungeru Area, Northwestern Nigeria

Please use this identifier to cite or link to this item: http://repository.futminna.edu.ng:8080/jspui/handle/123456789/17510

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DC Field	Value	Language
dc.contributor.author	Alabi, Garba, I, Danbat, U. Najime, T A. A	-
dc.date.accessioned	2023-01-19T07:53:16Z	-
dc.date.available	2023-01-19T07:53:16Z	-
dc.date.issued	2017-01-20	-
dc.identifier.citation	xx	en_US
dc.identifier.issn	XX	-
dc.identifier.uri	http://repository.futminna.edu.ng:8080/jspui/handle/123456789/17510	-
dc.description.abstract	Low grade schist belts are believed to have been formed as a resut of Pan-African orogeny characterized by deformaion, meamorphism and remobilization through three major processes. he schist are considered to be upper Proterozoic in age and consist of supercrustal rocks which has been folded into he migmatite-gniess complex. ten rock samples were collected from Zungeru area and analyzed using X-ray Diffracfrom Zungeruion (XRD), X-Ray Fluorescence technique and tin secion Perotrography.	en_US
dc.description.sponsorship	xx	en_US
dc.language.iso	en	en_US
dc.publisher	Minna, Journal of Geosciences	en_US
dc.relation.ispartofseries	xx;	-
dc.subject	Chemical Charateristics, Perogenic features, Metesedimentary rocks	en_US
dc.title	Compositional Characteristic and Petrogenic Feaures of Metasedimenary Rocks of Zungeru Area, Northwestern Nigeria	en_US
dc.title.alternative	xxx	en_US
dc.type	Article	en_US
Appears in Collections:	Geology

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